Congressional Serial Set Volume 5997
This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1911 edition. Excerpt: ...to an error in orthoclase, if all the alumina goes to that mineral, of 2.7 per cent, and the variation entrains others, especially in the estimation of the residual quartz. The compu...
Paperback: 372 pages
Publisher: RareBooksClub.com (June 26, 2012)
Product Dimensions: 7.4 x 0.8 x 9.7 inches
Format: PDF Text TXT book
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ed mineral composition of a rock is incorrect by multiples of the errors existing in the analysis, and these may be, in fact are, sometimes large. The normative or standard minerals, then, so far as the make-up of a rock is concerned, are partly real and partly conventional. They are, however, quantitative in application and give uniformity to the discussion of rocks. Upon them the quantitative classification is founded. First, all igneous rocks are divided into five classes, which are fixed within certain arbitrary limits by the ratios between the sake and the femic minerals. These classes are as follows: sal 7 I. Persalane: Extremely salic fern II. Dosalane: Dominantly salic fern 1 ' III. Salfemane: Equally salic and femic--§_f IV. Dofemane: Dominantly femic fem5-'7 Bal 1 V. Perfemane: Extremely femic fern 7 That is, the held between an entirely salic rock and one entirely femic is divided into five parts, each representing a definite range of variation. A rock containing more than seven-eighths of salic minerals to one-eighth femic is in the class persalane; one with less than seven-eighths salic to more than three-eighths femic falls under dosalane, and so on. A granite, for example, containing over 87.5 per cent of quartz and feldspar is placed in Class I; a peridotite with over 87.5 per cent of femic minerals belongs in Class V. Many basalts, gabbros, diorites, etc., contain salic and femic compounds in nearly equal proportions, and are therefore in Class III. From the norm of a rock its class can be determined at once, and in many cases a mere inspection...
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